Geochemical measurements of the Tasmanian Gateway from ODP Hole 189-1172A

Tectonic changes that produced a deep Tasmanian Gateway between Australia and Antarctica are widely invoked as the major mechanism for Antarctic cryosphere growth and Antarctic Circumpolar Current (ACC) development during the Eocene/Oligocene (E/O) transition (34-33 Ma). Ocean Drilling Program (ODP)...

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Bibliographic Details
Main Authors: Stickley, Catherine E, Brinkhuis, Henk, Schellenberg, Stephen A, Sluijs, Appy, Röhl, Ursula, Fuller, Michael D, Grauert, M, Huber, Matthew, Warnaar, Jeroen, Wiliams, Graham L
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
189-1172A
Carbon
organic
total
Carbonates
Coulometry
DEPTH
sediment/rock
DRILL
Drilling/drill rig
Grain size
mean
Isotope ratio mass spectrometry
Joides Resolution
Leg189
Ocean Drilling Program
ODP
Tasman Sea
δ13C
carbonate
δ18O
Antarc*
Antarctic
Antarctica
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.742605
https://doi.org/10.1594/PANGAEA.742605

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